Regenerative Step Pool Storm

Total Page:16

File Type:pdf, Size:1020Kb

Load more

Regenerative Step Pool Storm Conveyance (SPSC) – also known as Coastal Plain Outfalls Design Guidelines Draft Revision 3 Under Review Not for Distribution Home Port Farms - Immediately after i Home Port Farms - One year after construction Homeport Farms - Six years after construction Original : June 2009 Revision 1: August 2010 Revision 2: November 2010 Ron Bowen, P.E. Design Guidelines for Step Pool Storm Conveyance Anne Arundel County Government Department of Public Works, Bureau of Engineering Technical Advisory Committee This document was prepared by Hala Flores, P.E., with input from Dennis Mcmonigle and Keith Underwood. This document is maintained on the Anne Arundel County website and can be accessed through http://www.aacounty.org/DPW/Watershed/StepPoolStormConveyance.cfm. Updates and revisions to this document are reviewed by the Technical Advisory Committee as follows. Ronald E. Bowen, P.E., DPW Director Christopher J. Phipps, P.E., DPW, Chief Bureau of Engineering Kenneth Fleming, P.E., DPW, Assistant Chief Bureau of Engineering Ginger Ellis, DPW, Watershed Ecosystem, and Restoration Division Chief Keith Underwod, Underwood and Associates Hala Flores, P.E., DPW, Watershed Assessment and Planning Program Manager Janis Markusic, DPW, NPDES-MS4 Coordination/Ecosystem Assessment Program Manager Dennis McMonigle, DPW, Environmental Restoration Project Manager Christopher Soldano, OPZ, Deputy Director Richard Olsen, DPW, Infrastructure Management Division Elizabeth Burton, OPZ, Chief Engineer George Eberle, I&P, Assistant Director John Peacock, I&P, Code Enforcement Administrator Jim Stein, Vernon Murray, Chris Maex, and Charles Henney, AACO SCD Earl Reaves, I&P, County Forester Summary of Revisions: August 2010 Revision 1: (a) Added language to clarify when an SPSC system can and cannot be used as part of the ESD treatment train. November 2010 Revision 2: (a) Replaced the d50 cobble size definition with the d0 definition indicating that the cobble design size is the minimum allowable cobble size to be used rather than median stone size. (b) Added a clarification on the minimum and maximum allowable length of pools and riffles (c) Added a design checklist. (d) Added an inspection checklist. (e) Added guidance pertaining to sequence of construction and erosion and sediment control measures. April 2011 Revision 3: The MDE Stormwater guidelines prescribe that filtering systems shall fully drain within 72 hours, however unlike infiltration systems, no groundwater separation is specified for filtering system. Due to this, revision 3 eliminates the requirement for groundwater separation from the filtering system. However, to ensure that the filtering mechanism works as designed, the design water quality filter ponding depth in the pools, also known as seepage head, shall be available for storage during storm events and not inundated by seasonal ground water. Further, the pools shall drain down within 72 hours to their design levels. April 2011 Revision 3: Added horizontal and vertical setback requirements for SPSC systems. Added “Regenerative” to the practice name for consistency with EPA TMDL/WIP publications. April 2011 Revision 3: Width/Depth ratio for Riffle/Weir section shall not be less than 10W:1D. Further, pool depths shall not exceed 3 ft. Page 2 of 36 Step Pool Storm Conveyance (SPSC) Guidelines – Revision 2: November 2010 Design Guidelines for Step Pool Storm Conveyance Anne Arundel County Government Department of Public Works, Bureau of Engineering Important Note: This document features design guidelines and procedural steps to aid design engineers in sizing a Step Pool Storm Conveyance (SPSC) system. It is the responsibility of the design engineer to check the feasibility and acceptability for using these systems at their project site. SPSC can be used in lieu of stormdrains as roadside conveyance/attenuation systems. SPSC maybe used for peak flow management or steep slope stability treatment and are considered structural BMPs if they are sized to accommodate the State of Maryland volume control requirements specified in Chapter 2 of the State manual. In general, SPSC may be used as a structural stormwater management device to provide water quality treatment as part of the treatment train or at the downstream outfall after all Environmental Site Design (ESD) techniques have been exhausted to the Maximum Extent Practical (MEP) as dictated in the State of Maryland SWM manual. Under special circumstance, the SPSC may be used as part of the ESD when the design conforms to the criteria found in Chapter 5 (State of Maryland SWM Manual) for microbioretention or bio- swale and the general configuration conforms to the principles of ESD: using small-scale practices distributed uniformly around the site to capture runoff close to the source. While SPSC systems can be implemented on steep slopes, in no circumstance can water quality credit be claimed for SPSC segments with a longitudinal profile slope that exceeds 5 percent. Additionally for storm conveyance segments that exceed 5 % in longitudinal slope, it is imperative that a registered geotechnical engineer be enlisted to check the proposed design and its adequacy for use as a steep slope treatment measure. Introduction: SPSC are open-channel conveyance structures that convert, through attenuation ponds and a sand seepage filter, surface storm flow to shallow groundwater flow. These systems safely convey, attenuate, and treat the quality of storm flow. These structures utilize a series of constructed shallow aquatic pools, riffle grade control, native vegetation, and an underlying sand/woodchip mix filter bed media. The physical characteristics of the SPSC channel are best characterized by the Rosgen A or B stream classification types, where “bedform occurs as a step/pool, cascading channel which often stores large amounts of sediment in the pools associated with debris dams” (Rosgen, 1996). The pretreatment, recharge, and water quality sizing criteria presented in these guidelines follow closely the State of Maryland’s criteria for a typical stormwater filtering device. These structures feature surface/subsurface runoff storage seams and an energy dissipation design that is aimed at attenuating the flow to a desired level through energy and hydraulic power equivalency principles. SPSC structures can be designed to provide energy dissipation and extreme flood conveyance/attenuation functions, as well as recharge and water quality treatment in excess of ESD. The inherent energy dissipation achieved in the step pool design is directly linked through hydraulic design computations to reduced stream power and bank shear stresses in the receiving streams, thus satisfying more directly and effectively the State of Maryland’s channel protection requirement and additional local requirements for flood attenuation. The reduced energy and Page 3 of 36 Step Pool Storm Conveyance (SPSC) Guidelines – Revision 2: November 2010 Design Guidelines for Step Pool Storm Conveyance Anne Arundel County Government Department of Public Works, Bureau of Engineering velocity at the downstream end of these structures result in reduced channel erosion impacts commonly seen between conventional stormwater practice outfalls and ultimate receiving waters. SPSC structures are generally best suited in natural ravines and are the preferred method of storm water conveyance throughout the water train. ESD techniques such as alternative pavement, greenroofs, rooftop disconnections, vegetated swales, etc., should be considered and utilized to the MEP in the upstream area of a proposed SPSC system. A secondary benefit provided by the pools and plant material is to reduce flow velocity and enhance the removal of suspended particles and their associated nutrients and/or pollutants. Additionally, uptake of dissolved nutrients and adsorption of oils and greases by the plant material yield secondary water quality benefits above and beyond the benefits achieved through the primary water quality sand/woodchip mix filter. The design material and plant list featured within this document has been adapted to the Anne Arundel County coastal plain environment. The materials used within the SPSC, to the extent possible, are taken from the coastal plain. The sand media is quarried throughout the region and can be readily obtained. The boulders found in these systems are sandstone (e.g., bog iron, iron stone, ferracrete). Sandstone’s porosity, as well as its ability to retain water, allows it to naturalize quickly, providing habitat for ferns, moss, and other organisms that persist in these systems. While sandstone is the preferred material for use as boulders within these systems, granite may be substituted if sandstone availability is demonstrated to be of a concern. The use of other alternative boulder material must be approved by the Anne Arundel County reviewer and/or project manager. Under no circumstance is limestone or concrete permitted in the construction of SPSC systems. Construction specifications for the SPSC can be found in the Anne Arundel County Design Manual, Standard Specifications and Details for Construction document. General Design Situations SPSC structures consist of an open channel conveyance with alternating riffles and pools. These systems are best suited for ditches, outfalls, ephemeral and intermittent channels with longitudinal profile slopes that are less than 10%. However, the design can be easily adapted for sites where the slope exceeds 10 percent. For these sites, the size and quantity
Recommended publications
  • XS1 Riffle STA 0+27 Ground Points Bankfull Indicators Water Surface Points Wbkf = 26.9 Dbkf = 1.46 Abkf = 39.4 105

    XS1 Riffle STA 0+27 Ground Points Bankfull Indicators Water Surface Points Wbkf = 26.9 Dbkf = 1.46 Abkf = 39.4 105

    XS1 Riffle STA 0+27 Ground Points Bankfull Indicators Water Surface Points Wbkf = 26.9 Dbkf = 1.46 Abkf = 39.4 105 100 Elevation (ft) 95 90 0 102030405060 Horizontal Distance (ft) Team 1 Riffle STA 133 Ground Points Bankfull Indicators Water Surface Points Wbkf = 23.4 Dbkf = 1.48 Abkf = 34.6 105 100 Elevation (ft) 95 90 0 1020304050 Horizontal Distance (ft) XS3 Lateral Scour Pool STA 0+80.9 Ground Points Bankfull Indicators Water Surface Points Inner Berm Indicators Wbkf = 25.9 Dbkf = 1.73 Abkf = 44.7 105 Wib = 14 Dib = .93 Aib = 13.1 Elevation (ft) 90 0 90 Horizontal Distance (ft) Team 1 Lateral Scour Pool STA 211 Ground Points Bankfull Indicators Water Surface Points Inner Berm Indicators Wbkf = 26.8 Dbkf = 1.86 Abkf = 49.7 105 Wib = 15.2 Dib = .91 Aib = 13.7 100 Elevation (ft) 95 90 0 1020304050 Horizontal Distance (ft) XS2 Run STA 0+44.1 Ground Points Bankfull Indicators Water Surface Points Wbkf = 22.6 Dbkf = 1.96 Abkf = 44.4 105 100 Elevation (ft) 95 90 0 102030405060 Horizontal Distance (ft) Team 1 Run STA 151 Ground Points Bankfull Indicators Water Surface Points Wbkf = 24.2 Dbkf = 1.69 Abkf = 40.9 105 100 Elevation (ft) 95 90 0 1020304050 Horizontal Distance (ft) XS4 Glide STA 104.2 Ground Points Bankfull Indicators Water Surface Points Wbkf = 25.9 Dbkf = 1.62 Abkf = 42 106 Elevation (ft) 95 0 70 Horizontal Distance (ft) Team 1 Glide STA 236 Ground Points Bankfull Indicators Water Surface Points Inner Berm Indicators Wbkf = 20.8 Dbkf = 1.75 Abkf = 36.3 105 Wib = 15.7 Dib = .85 Aib = 13.3 100 Elevation (ft) 95 90 0 1020304050
  • Stream Restoration, a Natural Channel Design

    Stream Restoration, a Natural Channel Design

    Stream Restoration Prep8AICI by the North Carolina Stream Restonltlon Institute and North Carolina Sea Grant INC STATE UNIVERSITY I North Carolina State University and North Carolina A&T State University commit themselves to positive action to secure equal opportunity regardless of race, color, creed, national origin, religion, sex, age or disability. In addition, the two Universities welcome all persons without regard to sexual orientation. Contents Introduction to Fluvial Processes 1 Stream Assessment and Survey Procedures 2 Rosgen Stream-Classification Systems/ Channel Assessment and Validation Procedures 3 Bankfull Verification and Gage Station Analyses 4 Priority Options for Restoring Incised Streams 5 Reference Reach Survey 6 Design Procedures 7 Structures 8 Vegetation Stabilization and Riparian-Buffer Re-establishment 9 Erosion and Sediment-Control Plan 10 Flood Studies 11 Restoration Evaluation and Monitoring 12 References and Resources 13 Appendices Preface Streams and rivers serve many purposes, including water supply, The authors would like to thank the following people for reviewing wildlife habitat, energy generation, transportation and recreation. the document: A stream is a dynamic, complex system that includes not only Micky Clemmons the active channel but also the floodplain and the vegetation Rockie English, Ph.D. along its edges. A natural stream system remains stable while Chris Estes transporting a wide range of flows and sediment produced in its Angela Jessup, P.E. watershed, maintaining a state of "dynamic equilibrium." When Joseph Mickey changes to the channel, floodplain, vegetation, flow or sediment David Penrose supply significantly affect this equilibrium, the stream may Todd St. John become unstable and start adjusting toward a new equilibrium state.
  • The Form of a Channel

    The Form of a Channel

    23 GEOMORPHOLOGY 201 READER The bankfull discharge is that flow at which the channel is completely filled. Wide variations are seen in the frequency with which the bankfull discharge occurs, although it generally has a return period of one to two years for many stable alluvial rivers. The geomorphological work carried out by a given flow depends not only on its size but also on its frequency of occurrence over a given period of time. The flow in river channels exerts hydraulic forces on the boundary (bed and banks). An important balance exists between the erosive force of the flow (driving force) and the resistance of the boundary to erosion (resisting force). This determines the ability of a river to adjust and modify the morphology of its channel. One of the main factors influencing the erosive power of a given flow is its discharge: the volume of flow passing through a given cross-section in a given time. Discharge varies both spatially and temporally in natural river channels, changing in a downstream direction and fluctuating over time in response to inputs of precipitation. Characteristics of the flow regime of a river include seasonal variations in discharge, the size and frequency of floods and frequency and duration of droughts. The characteristics of the flow regime are determined not only by the climate but also by the physical and land use characteristics of the drainage basin. Valley setting Channel processes are driven by flow and sediment supply, although the range of channel adjustments that are possible are often restricted by the valley setting.
  • Flood Regime Typology for Floodplain Ecosystem Management As Applied to the Unregulated Cosumnes River of California, United States

    Flood Regime Typology for Floodplain Ecosystem Management As Applied to the Unregulated Cosumnes River of California, United States

    Received: 29 March 2016 Revised: 23 November 2016 Accepted: 1 December 2016 DOI: 10.1002/eco.1817 SPECIAL ISSUE PAPER Flood regime typology for floodplain ecosystem management as applied to the unregulated Cosumnes River of California, United States Alison A. Whipple1 | Joshua H. Viers2 | Helen E. Dahlke3 1 Center for Watershed Sciences, University of California Davis, CA, USA Abstract 2 School of Engineering, University of Floods, with their inherent spatiotemporal variability, drive floodplain physical and ecological pro- California Merced, CA, USA cesses. This research identifies a flood regime typology and approach for flood regime character- 3 Land, Air and Water Resources, University of ization, using unsupervised cluster analysis of flood events defined by ecologically meaningful California Davis, CA, USA metrics, including magnitude, timing, duration, and rate of change as applied to the unregulated Correspondence lowland alluvial Cosumnes River of California, United States. Flood events, isolated from the Alison A. Whipple, Center for Watershed 107‐year daily flow record, account for approximately two‐thirds of the annual flow volume. Sciences, University of California Davis, CA, USA. Our analysis suggests six flood types best capture the range of flood event variability. Two types Email: [email protected] are distinguished primarily by high peak flows, another by later season timing and long duration, Funding information two by small magnitudes separated by timing, and the last by later peak flow within the flood California Department of Fish and Wildlife, event. The flood regime was also evaluated through inter‐ and intra‐annual frequency of the iden- Grant/Award Number: E1120001; National Science Foundation, Grant/Award Number: tified flood types, their relationship to water year conditions, and their long‐term trends.
  • River Maintenance Methods Attachment

    River Maintenance Methods Attachment

    Joint Biological Assessment, Part II River Maintenance Methods Attachment River Maintenance Methods Attachment 1. Introduction Each strategy can be implemented using a variety of potential methods. The selection of methods depends upon local river conditions, reach constraints, and environmental effects. Method categories are described in section 3.2.3. Methods are the river maintenance features used to implement reach strategies to meet river maintenance goals. Methods can be used as multiple installations as part of a reach-based approach, at individual sites within the context of a reach- based approach, or at single sites to address a specific river maintenance issue that is separate from a reach strategy. The applicable methods for the Middle Rio Grande (MRG) have been organized into categories of methods with similar features and objectives. Methods may be applicable to more than one category because they can create different effects under various conditions. The method categories are: • Infrastructure Relocation or Setback • Channel Modification • Bank Protection/Stabilization • Cross Channel (River Spanning) Features • Conservation Easements • Change Sediment Supply A caveat should be added that, while these categories of methods are described in general, those descriptions are not applicable in all situations and will require more detailed, site-specific, analysis for implementation. It also should be noted that no single method or method combination is applicable in all situations. The suitability and effectiveness of a given method are a function of the inherent properties of the method and the physical characteristics of each reach and/or site. It is anticipated that new or revised methods will be developed in the future that also could be used on the Middle Rio Grande.
  • Restoring Meanders to Straightened Rivers 1

    Restoring Meanders to Straightened Rivers 1

    M ANUAL OF R IVE R R ESTO R ATION T ECHNIQUES Restoring Meanders to 1 Straightened Rivers 1.8 Restoring a meandering course to a high energy river ROTTAL BURN LOCATION – GLEN CLOVA, ANGUS, SCOTLAND NO36936919 DATE OF CONSTRUCTION – TWO PHASES - MAY/JUNE 2012 AND AUGUST 2012 Rottal Burn High energy, gravel LENGTH – 1,200m COST – £200,000 WFD Mitigation measure Waterbody ID 5812 Designation SAC Description Project specific Fish, Habitat, The Rottal Burn has a steep catchment of 17.05km² to its monitoring Macroinvertebrates, Plants, confluence with the River South Esk. The final 1km of the Birds, Morphology Rottal Burn between Rottal Lodge and its confluence with the River South Esk was realigned and straightened soon after the 1830s. In this final reach the steep catchment meets the South Esk glen. This reduces the gradient and results in deposition of bed material. The bed of the channelized burn was continually aggrading and sediment was sediment was being deposited at the confluence with the River South Esk. In response, sand, gravel owner of Rottal Estates, the fisheries trust saw an opportunity and cobbles had been dredged and and used for agricultural to improve the availability of fish habitat, and improve the embankments (up to 2.2m above field level) to reduce the overall habitat, by restoring the burn to a naturally functioning frequency of flooding of the surrounding fields. In 2003, the state and reconnecting it with its floodplain. This would support stretch was dredged again, destroying the existing habitat. the recovery of sustainable populations of Atlantic salmon, brown trout (Salmo trutta) and, in the long term, freshwater The River South Esk and its tributaries are designated for pearl mussel (which is dependant on salmonids for the Atlantic salmon (Salmo salar) and freshwater pearl mussel completion of its life cycle).
  • Modeling Forced Pool–Riffle Hydraulics in a Boulder-Bed Stream, Southern California ⁎ Lee R

    Modeling Forced Pool–Riffle Hydraulics in a Boulder-Bed Stream, Southern California ⁎ Lee R

    Geomorphology 83 (2007) 232–248 www.elsevier.com/locate/geomorph Modeling forced pool–riffle hydraulics in a boulder-bed stream, southern California ⁎ Lee R. Harrison , Edward A. Keller Department of Earth Science, University of California, Santa Barbara, Santa Barbara, CA 93106, USA Received 2 May 2005; received in revised form 13 February 2006; accepted 13 February 2006 Available online 11 July 2006 Abstract The mechanisms which control the formation and maintenance of pool–riffles are fundamental aspects of channel form and process. Most of the previous investigations on pool–riffle sequences have focused on alluvial rivers, and relatively few exist on the maintenance of these bedforms in boulder-bed channels. Here, we use a high-resolution two-dimensional flow model to investigate the interactions among large roughness elements, channel hydraulics, and the maintenance of a forced pool–riffle sequence in a boulder-bed stream. Model output indicates that at low discharge, a peak zone of shear stress and velocity occurs over the riffle. At or near bankfull discharge, the peak in velocity and shear stress is found at the pool head because of strong flow convergence created by large roughness elements. The strength of flow convergence is enhanced during model simulations of bankfull flow, resulting in a narrow, high velocity core that is translated through the pool head and pool center. The jet is strengthened by a backwater effect upstream of the constriction and the development of an eddy zone on the lee side of the boulder. The extent of flow convergence and divergence is quantified by identifying the effective width, defined here as the width which conveys 90% of the highest modeled velocities.
  • Sediment Impact Anaysis for the Lower Thames Flood Strategy Study

    Sediment Impact Anaysis for the Lower Thames Flood Strategy Study

    PROCEEDINGS of the Eighth Federal Interagency Sedimentation Conference (8thFISC), April2-6, 2006, Reno, NV, USA SEDIMENT IMPACT ANAYSIS FOR THE LOWER THAMES FLOOD STRATEGY STUDY Ian M Tomes, SE Area Flood Risk Manager, Environment Agency (Thames Region), Frimley, Surrey, UK, [email protected]; Oliver P. Harmar, Consultant Geomorphologist, Halcrow Group, Leeds, UK, [email protected]; Colin R. Thorne, Professor of Physical Geography, University of Nottingham, Nottingham, UK, [email protected], INTRODUCTION Sediment impact assessment was performed during the Lower Thames Flood Strategy Study to assess the geomorphological sustainability of river-bed re-profiling to reduce flood risk in the reach between Datchet and Teddington. The specific objectives of the sediment study were to: i. estimate how much sediment is likely to be deposited in, or eroded from, the study reach by flows up to and including long return interval flood events for ‘do minimum’ and ‘bed reprofiling’ options that would lower the bed by 0.5 to 1 m; ii. estimate an average annual rate of sedimentation for the ‘do minimum’ and ‘bed reprofiling’ options. MORPHOLOGY OF THE RIVER THAMES The study reach of the River Thames has the characteristics of a mature, lowland river with well developed meanders and reaches divided by stable, mid-channel islands. The movement of water and sediment along the river has been controlled by locks and weirs for over a century. These structures present obstructions to the natural movement of sediment and dredging was, historically, required to maintain a navigable channel. The banks along much of the navigable river have been stabilised by revetment and, therefore, the river is unable to adjust its planform.
  • Hydrometeorological Analysis and Forecasting of a 3-Day Flash-Flood- Triggering Desert Rainstorm

    Hydrometeorological Analysis and Forecasting of a 3-Day Flash-Flood- Triggering Desert Rainstorm

    https://doi.org/10.5194/nhess-2020-189 Preprint. Discussion started: 2 July 2020 c Author(s) 2020. CC BY 4.0 License. Hydrometeorological analysis and forecasting of a 3-day flash-flood- triggering desert rainstorm 5 Yair Rinat1,*, Francesco Marra1,2, Moshe Armon1, Asher Metzger1, Yoav Levi3, Pavel Khain3, Elyakom Vadislavsky3, Marcelo Rosensaft4, Efrat Morin1 (1) Institute of Earth Sciences, The Hebrew University of Jerusalem, Jerusalem, Israel (2) National Research Council of Italy, Institute of Atmospheric Sciences and Climate, CNR-ISAC, Bologna, Italy 10 (3) Israel Meteorological Service, Beit Dagan, Israel (4) Geological Survey of Israel, Jerusalem, Israel Correspondence to: Yair Rinat ([email protected]) Abstract: Flash floods are among the most devastating and lethal natural hazards. In 2018, three flash-flood episodes 15 resulted in 46 casualties in the deserts of Israel and Jordan alone. This paper presents the hydrometeorological analysis and forecasting of a substantial storm (25–27 Apr 2018) that hit an arid desert basin (Zin, ~1400 km2, southern Israel), claiming 12 human lives. Our aim was to: (a) spatially assess the severity of the storm, (b) quantify the time scale of the hydrological response, and (c) evaluate the available operational precipitation forecasting. Return periods of the storm's maximal rain intensities were derived locally, at 1-km2 resolution, using weather radar data and a novel statistical methodology. A high- 20 resolution grid-based hydrological model was used to study the intra-basin flash-flood magnitudes, which were consistent with direct information from witnesses. The model was further used to examine the hydrological response to different forecast scenarios.
  • Fordebris Flow Triggering Characteristics and Occurrence Probability After Extreme Rainfalls: Case Study in the Chenyulan Watershed, Taiwan

    Fordebris Flow Triggering Characteristics and Occurrence Probability After Extreme Rainfalls: Case Study in the Chenyulan Watershed, Taiwan

    forDebris flow triggering characteristics and occurrence probability after extreme rainfalls: case study in the Chenyulan watershed, Taiwan Jinn-Chyi Chen1, Jiang- Guo Jiang1, Wen-Shun Huang2, Yuan-Fan Tsai3 5 1Department of Environmental and Hazards-Resistant Design, Huafan University, Taipei 22301, Taiwan 2 Ecological Soil and Water Conservation Research Center, National Cheng Kung University, Tainan 70101, Taiwan 3Department of Social and Regional Development, National Taipei University of Education, Taipei 10671, Taiwan 10 Correspondence to: Jinn-Chyi Chen ([email protected]) ABSTRACT. Rainfall and other extreme events often trigger debris flows in Taiwan. This study examines the debris flow triggering characteristics and probability of debris flow occurrence after extreme rainfalls. The Chenyulan watershed, central Taiwan, which has suffered from the Chi-Chi 15 earthquake and extreme rainfalls, was selected as a study area. The rainfall index (RI) was used to analyze the return period and characteristics of debris flow occurrence after extreme rainfalls. The characteristics of debris flow occurrence included the variation in critical RI, threshold of RI for debris flow triggering, and recovery period, the time required for the lowered threshold to return to the original threshold. The variations in critical RI after extreme rainfall and the recovery period associated with RI 20 are presented. The critical RI threshold was reduced in the years following an extreme rainfall event. The reduction in RI as well as recovery period were influenced by the RI. Reduced RI values showed an increasing trend over time, and it gradually returned to the initial RI. The empirical relationship between the probability of debris flow occurrence (P) and corresponding return period (T) of the rainfall characteristics for areas affected by extreme rainfalls and affected by the Chi-Chi earthquake were 25 developed.
  • Developments in Stream Ecosystem ~ H E O R

    Developments in Stream Ecosystem ~ H E O R

    Developments in Stream Ecosystem ~heory' G. Wayne Minshall Department of Biology, Idaho State University, Pocatello, ID 83209, USA Kenneth W. 6umrnins2 Department sf Fisheries and Widlife, Oregon State University, CorvalEis, OW 9733 1, USA Robert C. Petersen Stream and Benthic Ecology Group, Institute of Limnology, University of bund, 5-22! 1 08 Lund, Sweden Colbert E. Cushing Environmental Sciences Department, Battelle Pacific-Northwest Laboratories, Richland, WA 99352, USA Dale A. Bruns EC & C Idaho, dnc., Environmental Sciences Section, ddaho Falls, ID 834 15, USA Forestry Sciences Laboratory, United States Forest Service, Corvalbis, 88 9733 1, USA and Robin L. Vannote Stroud Water Research Center, Academy of Natural Sciences si Philadelphia, Avondale, PA 198 1 1, USA Minshall, G.We, K. W. Curnrnins, R. C. Petersen, C. E. Cushing, B. A. Bruns, J.R. SedeH, and W. %.Vannote. 1985. Developments in stream ecosystem theory. Can. J.Fish. Aquat. Sci. 42: 1045-1055. Four significant areas ~f thought, (I) the holistic approach, (2) the linkage between streams and their terrestrial setting, (3) material cycling in open systems, and (4) biotic interactions and integration of community ecology principles, have provided a basis for the further development of stream ecosystem theory. The River Continuum Concept (RCC) represents a synthesis of these ideas. Suggestions are made for clarifying, expanding, and refining the RCC to encompass broader spatial and temporal scales. Factors important in this regard include climate and geology, tributaries, location-specific lithology and geo- morphology, and long-term changes imposed by man. It appears that most riverine ecosystems can be accolr~modatedwithin this expanded conceptual framework and that the WCC continues to represent a useful paradigm for understanding and comparing the ecology of streams and rivers.
  • Some Actions for Sustainable Development – Sri Lanka

    Some Actions for Sustainable Development – Sri Lanka

    Water-centric Inter-linkages Some Case Studies in Sri Lanka S.B Weerakoon1 - Water with Floods, Climate, Energy Cho Thanda Nyunt2 - Water with Climate Change Yoshimitsu Tajima3 - Water with Coastal Environment 1University of Peradeniya, Sri Lanka 2University of Tokyo, Japan 3University of Tokyo, Japan Rainfall Forecasting and Flood Inundation along the Lower Reach of Kelani River Basin under Changing Climate S.B Weerakoon1, Srikantha Herath2 , Gouri De Silva1 1Department of Civil Engineering, University of Peradeniya, Peradeniya, Sri Lanka 2United Nations University, Shibuya-ku, Tokyo, Japan Elevation distribution Flood inundation in Colombo(DEM) and suburbs create heavy economic damages 4 Kelani River Basin Region – Wet Zone Total Basin Area – 2,230 km2 Uppermost Elevation – 2,250 m Length of the River – 192 km Average Annual Rainfall – 2,400 mm Peak flow – 800-1500 m3/s Vegetation cover Upper basin – Tea, rubber, grass and forest Lower basin – heavily urbanized 1. Weather forecasting for flood warning Rainfall forecasting using downscaling of 72 hr climate model data by Weather Research and Forecasting (WRF) model - to provide early warning on rainfall and floods Application of Weather Research and Forecasting model (WRF model) Nesting option – 135/45/15/5 (4050 ×4050 / 1530 ×1395 / 465 ×465 / 245 ×260 ) with푘푚 input resolution푘 푚of 10 minutes 푘푚 푘푚 푘푚 Input data downloaded from NCAR web site WRF – short term rainfall forecasting Calibration – 21st November 2005 Validation – 27th and 28th April 2008, and 30th, 31st May and 1st June 2008 Justification Mean Absolute Model Error percentage % = × 푺푺푺푺푺푺푺푺푺 푹푺푺푹푹� − 푶푶푶푺푶푶 푹푺푺푹푹� 푴푴푴푴 ퟏퟏퟏퟏ 푶푶푶푺푶푶 푹푺푺푹푹� Calibration and validation Calibration Difference between WRF predictions and observed rainfall for the date 21st November 2005 Validation Difference between WRF predictions and observed rainfall for the date 27th April 2008 Validation Difference between WRF predictions and observed rainfall for the date 31st May 2008 Difference between WRF predictions and observed rainfall for the date 1st June 2008 2.